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Jepang · Stratovolkan

Mikura-jima

Mikurajima

Tipe
Stratovolkan
Ketinggian
851 m
Letusan terakhir
-4100
Mikura-jima
Foto: Izawa Ryu · CC BY-SA 4.0 · Wikimedia Commons
Tipe
Stratovolkan
Negara
Jepang
Wilayah
Pasifik Barat Laut / Izu Volcanic Arc
Ketinggian
851 m
Koordinat
33.874, 139.602
Letusan terakhir
-4100
Kondisi tektonik
Zona subduksi / Kerak samudra (< 15 km)
Bentuk lahan
Komposit
Batuan utama
Basal / Pikrobasal
Ringkasan geologi

Mikurajima is a small steep-sided island located between the more well-known Miyakejima and Hachijojima volcanoes. Oyama forms the summit of the basaltic-to-andesitic island, which is surrounded by cliffs and dissected on the southern-to-eastern sides. The sparsely populated island consists of a large stratovolcano with lava domes on the SE side. Several small sea stacks are located immediately offshore. Growth of the stratovolcano took place until about 7,000 years ago, and the latest activity occurred about 6,000 years ago, when explosive eruptions and pyroclastic surges accompanied lava dome growth.

Ringkasan Wikipedia

Ringkasan Inggris

Mikura-jima (御蔵島) is an inhabited volcanic Japanese island in the Pacific Ocean. The island is administered by Tōkyō Metropolis and is located approximately 200 kilometres (120 mi) south of Tokyo and 19 kilometres (12 mi) south-southeast of Miyakejima. It is one of the Izu Seven Islands group of the seven northern islands of the Izu archipelago. Mikurashima is administratively part of Mikurashima Village under Miyake Subprefecture of Tokyo Metropolis. As of 2009, the island's population was 351. Mikura-shima is also within the boundaries of the Fuji-Hakone-Izu National Park.

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Riwayat letusan

2 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu · Gunakan tombol panah untuk berpindah batang, Enter untuk membuka
5050 SM~4955 SM · 1 letusan · VEI maks. ?4195 SM~4100 SM · 1 letusan · VEI maks. ?5050 SM4860 SM4575 SM4385 SM4195 SM

Garis waktu rinci

  1. 4100 SM (±100 tahun)VEI ?Perkiraan geologi
    4100 SM – akhir tidak diketahui
    Tsubunegamori & Yasukajigamori domes
  2. 5050 SMVEI ?Perkiraan geologi
    5050 SM – akhir tidak diketahui

Gunung api terdekat

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.